EXTENDING THE VOSTOK ICE-CORE RECORD OF PALEOCLIMATE TO THE PENULTIMATE GLACIAL PERIOD

被引：425

作者：

JOUZEL, J

BARKOV, NI

BARNOLA, JM

BENDER, M

CHAPPELLAZ, J

GENTHON, C

KOTLYAKOV, VM

LIPENKOV, V

LORIUS, C

PETIT, JR

RAYNAUD, D

RAISBECK, G

RITZ, C

SOWERS, T

STIEVENARD, M

YIOU, F

YIOU, P

机构：

[1] ST PETERSBURG ARCTIC & ANTARCTIC RES INST,ST PETERSBURG 199226,RUSSIA

[2] CNRS,GLACIOL & GEOPHYS ENVIRONNEMENT LAB,F-38402 ST MARTIN DHERES,FRANCE

[3] UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 02882

[4] MOSCOW GEOG INST,MOSCOW 109017,RUSSIA

[5] CTR SPECTROMETRIE NUCL & SPECTROMETRIE MASSE,F-91405 ORSAY,FRANCE

来源：

NATURE | 1993年 / 364卷 / 6436期

关键词：

D O I：

10.1038/364407a0

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

The ice-core record of local temperature, dust accumulation and air composition at Vostok station, Antarctica, now extends back to the penultimate glacial period (approximately 140-200 kyr ago) and the end of the preceding interglacial. This yields a new glaciological timescale for the whole record, which is consistent with ocean records. Temperatures at Vostok appear to have been more uniformly cold in the penultimate glacial period than in the most recent one. Concentrations of CO2 and CH4 Correlate well with temperature throughout the record.

引用

页码：407 / 412

页数：6

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[41] ICE CORES AND CLIMATIC CHANGE [J].